65.0525,-106.8583,0,076GSE0006,outcrop,Dox 0759,076G02,Slave,Au,Reconnaissance,1098500,,22-Oct-97,Source: Assessment Report,500 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada.  Administrative Region:  District of Mackenzie.  The latitude and longitude given are taken from the sample site of the map accompanying assessment report 061344.  ,"The Beech showing is approximately 290 miles NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.  ",,
65.2467,-106.6156,0,076GSE0009,outcrop,Ira,076G02,Slave,Cu-Ag-Au-Mo,Undrilled,,,6-Apr-98,Source: Assessment Report,30 Metres,The latitude and longitude given are taken from the best sample site of the map accompanying assessment report 081682.  ,"The IRA showing is approximately 500 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.  ",Within 1860 acres that surround the IRA showing the regional metamorphic grade is transitional from upper greenschist (NW) to lower amphibolite facies (SE). Assessment report 081682 notes that the cordiorite-staurolite isograd passes through this area. Contact metamorphism is evidenced by a narrow zone of migmitization and partial assimilation near the intrusive contacts.  The intrusive contact and major quartz vein are offset by fault structures. Offsets resulted in a southward displacement (100 m) of the mineralized quartz vein. ,
65.2,-106.5586,0,076GSE0010,outcrop,Beech 1,076G02,Slave,Au-Cu,Undrilled,,,6-Apr-98,Source: Assessment Report,30 Metres,The latitude and longitude given are taken from the best sample site of the map accompanying assessment report 082993.  ,"The Beech 1 showing is approximately 500 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.  ",Archean aged sediments and volcanic rocks grade from upper greenschist to upper amphibolite facies. ,
65.1614,-106.5408,0,076GSE0011,outcrop,Beech,076G02,Slave,Au-Cu,Undrilled,,,6-Apr-98,Source: Assessment Report,30 Metres,The latitude and longitude given is taken from the best sample site of the map accompanying assessment report 082993.  ,"The Beech showing is approximately 500 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.  ",Metamorphic range of the area is upper greenschist to upper amphibolite ,
65.0811,-106.8703,0,076GSE0012,outcrop,Casey Lake,076G02,Slave,Zn,Reconnaissance,,,7-Apr-98,Source: Assessment Report,30 Metres,The latitude and longitude given are taken from the best sample site of the map accompanying assessment report 081656.   ,"The Beech showing is approximately 465 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.  ",Cordierite and staurolite isograd trends through the area.,
65.0753,-106.9033,0,076GSE0013,outcrop,GM7,076G02,Slave,Zn,Reconnaissance,,,7-Apr-98,Source: Assessment Report,30 Metres,The latitude and longitude given are taken from the best sample site of the map accompanying assessment report 081656. ,"The Beech showing is approximately 465 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter. ",strike 120-130 dip 70-75 E  Metavolcanic rocks occur as a series of fault bounded lenses ,
65.0886,-107.1386,0,076GSW0010,outcrop,Needle Lake,076G03,Slave,Au,Drilled,,,3-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude of the showing is taken from the site of the highest gold value in the showing area.  ,"The Needle Lake area is south and east of Malley Rapids on the Back River. The area is approximately 455 km NE of Yellowknife, NT and approximately 185 km SE of the Lupin gold mine at Contwoyto Lake. Access to the area is by ski- or float-equipped fixed wing aircraft, or by helicopter.",At least four periods of deformation have affected the Yellowknife Supergroup. Metamorphic grade in the Back River Region ranges from sub-greenschist to upper amphibolite facies. In the Needle Lake area the general metamorphic grade is upper greenschist but within 300 m of the Regan Intrusive Suite plutons the grade increases to lower amphibolite grade and are increasingly deformed.,
65.0928,-107.2294,0,076GSW0011,outcrop,Moth Valley,076G03,Slave,Au,Undrilled,,,5-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude of the showing is taken from the site of the highest assay value in the showing area.   ,"The Moth Valley area is south and east of Malley Rapids on the Back River. The area is approximately 455 km NE of Yellowknife, NT and approximately 180 km SE of the Lupin gold mine at Contwoyto Lake. Access to the area is by ski- or float-equipped fixed wing aircraft, or by helicopter. ",The Moth Valley iron formation is folded into moderate to steeply west plunging isoclinal folds and have axial planes that plunge west. The Beechey Lake Group rocks in the Moth Valley area are folded into a large west trending synform which has a range in width from 600 m to 1.5 km and is approximately 4 km in length. Iron formations within the sequence vary in width from less than 1 m to 100 m in the fold noses. ,
65.0453,-107.1681,0,076GSW0012,outcrop,Gollum Lake,076G03,Slave,Au,Reconnaissance,,,5-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude of the showing is taken from a single sample site that comprises the showing. ,"The Gollum Lake area is south and east of Malley Rapids on the Back River. The area is approximately 455 km NE of Yellowknife, NT and approximately 185 km SE of the Lupin gold mine at Contwoyto Lake. Access to the area is by ski- or float-equipped fixed wing aircraft, or by helicopter.  ",A shear zone exists parallel along the contact of a granitic pluton and sediment package.,
65.0453,-107.1681,0,076GSW0013,outcrop,North Gollum Lake,076G03,Slave,Au,Reconnaissance,,,5-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude of the showing is from the area with the highest assay values.  ,"The North Gollum Lake area is south and east of Malley Rapids on the Back River. The area is approximately 455 km NE of Yellowknife, NT and approximately 185 km SE of the Lupin gold mine at Contwoyto Lake. Access to the area is by ski- or float-equipped fixed wing aircraft, or by helicopter.  ",,
65.0206,-107.2344,0,076GSW0014,outcrop,Phaedrus Lake,076G03,Slave,Au,Reconnaissance,,,5-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude of the showing is taken from the site of the highest assay value. ,"The Phaedrus Lake area is south and east of Malley Rapids on the Back River. The area is approximately 455 km NE of Yellowknife, NT and approximately 185 km SE of the Lupin gold mine at Contwoyto Lake. Access to the area is by ski- or float-equipped fixed wing aircraft, or by helicopter.  ",,
65.0986,-107.115,0,076GSW0015,outcrop,North Jaeger Lake,076G03,Slave,Au,Reconnaissance,,,5-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given are for the site of the highest gold value in the showing area which consists of 3 rock grab samples.,"North Jaeger Lake is a on the NE shore of a small lake north of Jaeger Lake. Dwg. 0605.N-10 shows the location and sample sites for the area. North Jaeger Lake is 1.5 km NE of the Needle Lake showing. The Needle Lake area is south and east of Malley Rapids on the Back River. The area is approximately 455 km NE of Yellowknife, NT and approximately 185 km SE of the Lupin gold mine at Contwoyto Lake. Access to the area is by ski- or float-equipped fixed wing aircraft, or by helicopter. ",,
65.0956,-107.2942,0,076GSW0016,outcrop,BLS-3,076G03,Slave,Au,Reconnaissance,,,6-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given are from the site of the highest gold value in the showing area.,"The BLS-3 Showing is centred approximately 7.3 km from the Needle Lake showing. Dwg. 0605.N-10 shows the location and sample sites for the area. The Needle Lake area is south and east of Malley Rapids on the Back River. The area is approximately 455 km NE of Yellowknife, NT and approximately 185 km SE of the Lupin gold mine at Contwoyto Lake. Access to the area is by ski- or float-equipped fixed wing aircraft, or by helicopter.  ",,
65.2142,-107.3328,0,076GSW0017,outcrop,Feather Lake,076G03,Slave,Au,Undrilled,,,6-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given are from the site of the highest gold value in the showing area. ,"The Feather Lake Showing is located along the Back River in the NW quadrant of NTS map 076G/03. This area has also been called Malley Rapids. The property is located approximately 455 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft or by helicopter.","Yellowknife Supergroup rocks in the area are folded into a steeply dipping, NW striking, regional scale anticlinorium that plunges to the SE. The Beechey Lake Group rocks within this anticlinorium are in a shallow SE plunging synform that is complexly folded.",
65.2089,-107.3067,0,076GSW0018,outcrop,Bor Lake,076G03,Slave,Au,Reconnaissance,,,9-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given are for the highest gold value in the showing area. ,"The Bor Lake Showing is located along the Back River in the NW quadrant of NTS map 076G/03. This area has also been called Malley Rapids. The property is located approximately 455 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft or by helicopter. ",,
65.2006,-107.2781,0,076GSW0019,outcrop,Bor Lake SE,076G03,Slave,Au,Reconnaissance,,,9-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given are from the site of the highest gold value in the showing area. ,"The Bor Lake SE Showing is located along the Back River in the NW quadrant of NTS map 076G/03. This area has been called Malley Rapids previously. The property is located approximately 455 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft or by helicopter.  ",
65.2483,-107.2992,0,076GSW0020,outcrop,Zone F,076G03,Slave,Au,Undrilled,,,9-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given are from the site of the highest gold value in the showing area. ,"The Zone F Showing is located at the top of the NW quadrant of NTS map 076G/03. This area has been called Malley Rapids previously. The property is located approximately 455 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft or by helicopter.   ",
65.2269,-107.1161,0,076GSW0021,outcrop,Bee,076G03,Slave,Au,Undrilled,,,9-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given are from the site of the highest gold value in the showing area. ,"The Bee area is located in the NNE quadrant of NTS map 076G/03. The property is located approximately 464 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft or by helicopter. ",
65.2319,-107.1603,0,076GSW0022,outcrop,Robbs Pond,076G03,Slave,Au,Reconnaissance,,,10-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given is the site of the highest gold value.,"The Robbs Pond area is located in the NNE quadrant of NTS map 076G/03. The property is located approximately 464 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft or by helicopter.  ",
65.2006,-107.0786,0,076GSW0023,outcrop,Dox 2380,076G03,Slave,Au,Reconnaissance,,,10-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given is from the site of the single gold sample that comprises this showing. ,"The sample area is located in the NNE quadrant of NTS map 076G/03. The property is located approximately 464 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft or by helicopter.  ",
65.2056,-107.1011,0,076GSW0024,outcrop,Dox 2384,076G03,Slave,Au,Reconnaissance,,,10-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given are for the single sample site (gold) that comprises this  showing. ,"The sample area is located in the NNE quadrant of NTS map 076G/03. The property is located approximately 464 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft or by helicopter.  ",
65.1869,-107.0494,0,076GSW0025,outcrop,Dox 2372,076G03,Slave,Au,Reconnaissance,,,12-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given are from the single sample site (gold) that comprises this  showing.  ,"The sample area is located in the NNE quadrant of NTS map 076G/03. The property is located approximately 464 km NE of Yellowknife, NT. Access is by float or ski eqipped fixed wing aircraft or by helicopter.  ",
65.2108,-107.1281,0,076GSW0026,outcrop,HG-106,076G03,Slave,Au,Reconnaissance,,,18-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given are taken from the single sample site that comprises this showing.,"The area of the sample site is approximately 475 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.",
65.2058,-107.2169,0,076GSW0027,outcrop,FG-74,076G03,Slave,Au,Reconnaissance,,,18-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given is from the single sample site that comprises this showing.,"The area of the sample site is approximately 475 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter",
65.2167,-107.7167,0,076GSW0003,outcrop,Hunt,076G04,Slave,Cu-Zn-Pb-Co-As,Reconnaissance,442500,,22-Oct-97,To Be Determined,Unknown,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada.  Administrative Region:  District of Mackenzie.  Location of showing determined from Cu Commodity File.,The Hunt Showing is approximately 460 km NE of Yellowknife NT. Access is by ski or float equipped fixed wing aircraft or by helicopter.,
65.0778,-107.6106,0,076GSW0007,outcrop,Fidler Lake,076G04,Slave,Au,Undrilled,1098600,,22-Oct-97,Source: Assessment Report,500 Metres,Latitude and longitude are from the best sample site within the showing area.,"The Fidler Lake showing is approximately 420 km NW of Yellowknife, NT. Access is by ski or float equipped fixed wing aircraft or by helicopter.",
65.2067,-107.9592,0,076GSW0008,outcrop,Ack,076G04,Slave,Au,Drilled,1098700,076G04AU 002,22-Oct-97,Source: Assessment Report,100 Metres,The latitude and longitude for this showing is from the site of the highest gold value.,The Ack showing is located approximately 2 km SSW of Uist Lake and 445 km NE of Yellowknife NT. Access to the area is by ski or float equipped fixed wing aircraft.,"Tight folding at the outcrop scale with folds plunging NW and SW suggesting refolding at a regional scale. Assessment reports list this as ""low to moderate metamorphic grade""."
65.0056,-107.5261,0,076GSW0035,outcrop,Alb,076G04,Slave,Au,Drilled,,,20-Apr-98,Source: Assessment Report,500 Metres,The lat and long are from the approximate location of DDH 84-01. The map it was taken from is a very poorly photocopied map.,"The Alb showing is located in the SE corner of NTS sheet 076/04 approximately 450 km from Yellowknife, NT. Access is by fixed wing ski or float equipped aircraft or by helicopter.",
65.0711,-107.57,0,076GSW0036,outcrop,Barrel,076G04,Slave,Au,Undrilled,,,23-Apr-98,Source: Assessment Report,100 Metres,Latitude and longitude are from the best sample site within the showing area. ,"The Barrel showing is approximately 420 km NW of Yellowknife, NT. Access is by ski or float equipped fixed wing aircraft or by helicopter. ",
65.1053,-107.6778,0,076GSW0037,outcrop,Algood,076G04,Slave,Au,Drilled,,,23-Apr-98,Source: Assessment Report,30 Metres,Latitude and longitude are from the #1 showing area.,"The Algood showing is approximately 440 km NE of Yellowknife, NT, and approximately 3.75 km N of Fidler Lake. Access is by ski or float equipped fixed wing aircraft or by helicopter.",
65.0328,-107.6758,0,076GSW0038,outcrop,South Fidler Lake,076G04,Slave,Au,Drilled,,,30-Apr-98,Source: Assessment Report,30 Metres,The showing location is from the area of highest assay values.,"The South Fidler Lake showing is approximately 460 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",The Back River Group (on a regional scale) is highly folded and has been affected by granitoid intrusions. Regional and contact metaqmorphism is variable from greenschist facies to middle amphibolite facies.
65.0836,-107.6939,0,076GSW0039,outcrop,Narrow Lake,076G04,Slave,Au,Undrilled,,,5-May-98,Source: Assessment Report,100 Metres,The showing location is from highest insitu gold value from assessment report 082625.,"The Narrow Lake showing is approximately 460 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis. ",,"Conjugate fault trends N10W, 2 metres wide"
65.0922,-107.7211,0,076GSW0040,outcrop,MG1,076G04,Slave,Au,Undrilled,,,6-May-98,Source: Assessment Report,30 Metres,The Showing location is determined by the highest assay value from assessment report 082624,"The MG1 showing is approximately 460 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis. ",,
65.1078,-107.7583,0,076GSW0041,outcrop,Grid 4,076G04,Slave,Au,Reconnaissance,,,7-May-98,Source: Assessment Report,100 Metres,The Showing location is from the site of the highest assay value from assessment report 082625 ,"The Grid 4 showing is approximately 460 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis. ",,
65.0878,-107.8744,0,076GSW0042,outcrop,Grid 5,076G04,Slave,Au,Undrilled,,,8-May-98,Source: Assessment Report,30 Metres,The showing location is from the sample site with the highest assay value.,"The Grid 5 showing is approximately 460 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis. ",,
65.1039,-107.8314,0,076GSW0043,outcrop,Grid 2,076G04,Slave,Au,Drilled,,,8-May-98,Source: Assessment Report,30 Metres,The latitude and longitude given are for the highest assay value of the showing area. Three drill holes were drilled within the showing but no samples had assay values above cutoff.,"The Grid 2 showing is approximately 460 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis. ",,
65.0922,-107.78,0,076GSW0044,outcrop,Grid 3,076G04,Slave,Au,Undrilled,,,11-May-98,Source: Assessment Report,100 Metres,The latitude and longitude given are for the highest assay value of the showing area.,"The Grid 3 showing is located on the eastern shore of Regan Lake approximately 460 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis. ",,
65.1289,-107.5861,0,076GSW0045,outcrop,Kate Zone,076G04,Slave,Au,Reconnaissance,,,12-May-98,Source: Assessment Report,30 Metres,The latitude and longitude given are for the highest assay value of the showing area.,"The Kate Zone showing is located approximately 6 km south of Fidler Lake approximately 470 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",,
65.1953,-107.6617,0,076GSW0046,outcrop,Twin Lake East,076G04,Slave,Au,Reconnaissance,,,12-May-98,Source: Assessment Report,100 Metres,The latitude and longitude given are for the highest assay value of the showing area.,"The Twin lakes East showing is located in the NE corner of NTS map 076G approximately 480 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",,
65.1142,-107.8544,0,076GSW0047,outcrop,Fire,076G04,Slave,Au,Reconnaissance,,,12-May-98,Source: Assessment Report,100 Metres,Latitude and longitude are from the single sample site from assessment report 083298.,"The Fire Showing is located at the NE tip of Regan Lake in the NE corner of NTS map 076G approximately 450 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",,
65.1189,-107.8997,0,076GSW0048,outcrop,Syn,076G04,Slave,Au,Reconnaissance,,,13-May-98,Source: Assessment Report,100 Metres,Latitude and longitude are from a single sample site as given in Assessment Report 083298.,"The Syn showing is located approximately 450 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",,
65.1322,-107.9433,0,076GSW0049,outcrop,A0902,076G04,Slave,Zn-Cu,Reconnaissance,,,14-May-98,Source: Assessment Report,100 Metres,Latitude and longitude are taken from the single sample site from assessment report 081610,"The A0902 Showing is located approximately 450 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",,
65.1558,-107.9028,0,076GSW0050,outcrop,A0865,076G04,Slave,Au,Reconnaissance,,,14-May-98,Source: Assessment Report,100 Metres,Latitude and longitude are taken from the single sample site from assessment report 081610,"The A0865 showing is located approximately 450 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",,
65.1558,-107.9625,0,076GSW0051,outcrop,A0912 & A0913,076G04,Slave,Au-Cu,Reconnaissance,,,14-May-98,Source: Assessment Report,100 Metres,This showing consists of two samples only.,"The A0912 & A0913 showing is located approximately 450 km NE of Yellowknife, NT. Access to the area is by fixed wing aircraft equipped with either floats or skis.",,
65.2289,-107.9483,0,076GSW0052,outcrop,Uist Lake,076G04,Slave,Au,Reconnaissance,,,19-May-98,Source: Assessment Report,100 Metres,This showin consists of a  single sample listed in assessment report 081610 ,The Uist Lake showing is located on the south shore of Uist Lake approximately 447 km NE of Yellowknife NT. Access is by float or ski equipped fixed wing aircraft or by helicopter.,,
65.2089,-107.9311,0,076GSW0053,outcrop,DC Grid,076G04,Slave,Au,Undrilled,,,19-May-98,Source: Assessment Report,100 Metres,,The DC Grid is located approximately 445 km NE of Yellowknife NT. Access is by ski or float equipped fixed wing aircraft or by helicopter.,The iron formation grades into amphibolitic argillites and amphibolitic chlorite schists. Felsic plutons in the Uist Lake area intrude the sediments and produce amphibolite grade metamorphism.,
65.1939,-107.9208,0,076GSW0054,outcrop,H Grid,076G04,Slave,Au,Undrilled,,,19-May-98,Source: Assessment Report,100 Metres,Location is from the best sample result.,The H Grid is located approximately 440 km NE of Yellowknife NT. Access is by ski or float equipped fixed wing aircraft or by helicopter.,Felsic plutons in the Uist Lake area intrude the sediments and produce amphibolite grade metamorphism.,
65.1628,-107.9033,0,076GSW0055,outcrop,As Grid,076G04,Slave,Au,Undrilled,,,19-May-98,Source: Assessment Report,100 Metres,Location determined by sample site highest assay values.,The As Grid is located approximately 440 km NE of Yellowknife NT. Access is by ski or float equipped fixed wing aircraft or by helicopter.,Felsic plutons in the Uist Lake area intrude the sediments and produce amphibolite grade metamorphism.
65.1189,-107.7425,0,076GSW0056,outcrop,Soc,076G04,Slave,Au,Drilled,,,20-May-98,Source: Assessment Report,100 Metres,The Soc Showing includes the FFB Showing (076GSW0057) which is located approximately 700 m to the west.,"The Soc showing is located approximately 450 km NE of Yellowknife NT. Access to the area is via ski or float equipped fixed wing aircraft onto larger lakes, or aircraft with tundra tires can access some of the local eskers.",
65.1206,-107.7564,0,076GSW0057,outcrop,FFB,076G04,Slave,Au,Drilled,,,21-May-98,Source: Assessment Report,100 Metres,This showing is part of the Soc showing. For further information and references see Normin ID # 076GSW0056,,
65.1325,-107.7892,0,076GSW0058,outcrop,Main,076G04,Slave,Au,Drilled,,,21-May-98,Source: Assessment Report,100 Metres,The Main Showing includes the West Main Showing (076GSW0059) which is located approximately 750 m to the west.,"The Main showing is located approximately 450 km NE of Yellowknife NT. Access to the area is via ski or float equipped fixed wing aircraft onto larger lakes, or aircraft with tundra tires can access some of the local eskers.",
65.1389,-107.7978,0,076GSW0059,outcrop,West Main,076G04,Slave,Au,Drilled,,,21-May-98,Source: Assessment Report,100 Metres,This showing is part of the Main showing. For further information and references see Normin ID # 076GSW0058,,
65.1069,-107.96,0,076GSW0060,outcrop,Fire 10,076G04,Slave,Zn-Pb-Ag,Reconnaissance,,,25-May-98,Source: Assessment Report,100 Metres,The latitude and longitude are from the highest assay value sample site.,"The Fire 10 showing is approximately 450 km NE of Yellowknife, NT. Access is by float or ski equipped fixed wing aircraft.",
65.2375,-107.9897,0,076GSW0061,outcrop,Uist 1,076G04,Slave,Au,Undrilled,,,27-May-98,Source: Assessment Report,100 Metres,Latitude and longitude for the showing are from the site of highest gold values. The Uist 1 showing consists of two grid/showing areas called Wallys showing and Eds showing.,"The Uist 1 showing is located along the south shore of Uist Lake approximately 430 km NE of Yelloweknife, NWT. The area is accessible by float or ski equipped fixed wing aircraft or by helicopter.",Beechey Lake group rocks are metamorphosed to at least greenschist facies - biotite grade.  Four phases of deformation are documented for the region but only three are evidenced on the showing property.
65.2342,-107.9742,0,076GSW0062,outcrop,Eds Showing,076G04,Slave,Au,Undrilled,,,29-May-98,Source: Assessment Report,100 Metres,This showing is part of the Uist 1 showing. For further information and references see Normin ID # 076GSW0061.,,
65.3231,-107.6208,0,076GSW0001,outcrop,Musk,076G05,Slave,Zn-Pb-Cu-Ag-Au-Ni,Resources Calculated,,,22-Oct-97,Source: Assessment Report,100 Metres,"The Musk Showing has been listed as having drill indicated reserves of 387,000 tons grading 1.2% Cu, 1.39% Pb, 10.38% Zn, 10.87 oz/ton Ag and 0.049 oz/ton Au. This is based on a total of 36 diamond drill holes totalling 3331 m.","The Musk Showing is accessable by float or ski equipped plane or helicopter. It is located approximately 460 km northeast from Yellowknife, NWT. An esker suitable for wheeled aircraft is located 6.5 km south.",The deposits are located on the limb of a steeply inclined NW trending fold which is marked by a strong S1 foliation. A crenulation cleavage is related to a second folding event.
65.4947,-107.7622,0,076GSW0033,outcrop,Gaet,076G05,Slave,Au,Undrilled,,,15-Apr-98,Source: Assessment Report,500 Metres,The latitude and longitude given are taken from the sample sites of the map accompanying assessment report 083071. The area discussed is the central area of a grid that is 3 km long by 2 km wide and has the best assay results.,"The general area of the sample site is approximately 450 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.  ",
65.49,-107.8,0,076GSW0034,outcrop,Gaet 4,076G05,Slave,Au,Reconnaissance,,,16-Apr-98,Source: Assessment Report,30 Metres,The latitude and longitude given are taken from a single sample site of map 1 accompanying assessment report 083071.  ,"The general area of the sample site is approximately 450 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter. ",
65.3972,-107.6881,0,076GSW0063,outcrop,IM 1,076G05,Slave,Au,Undrilled,,,1-Jun-98,Source: Assessment Report,100 Metres,"The Triangle Lake Showing is part of the IM 1 Showing (ID 076GSW0063). The IM 1 Showing is approximately 700 m NW along strike. The latitude and longitude of the showing was determined by the highest assay value reported.  Gold mineralization occurs with disseminations and beds of pyrrhotite in siliceous, amphibolitic iron formatioms.","The IM 1 showing is located approximately 460 km NE of Yellowknife, NT. Access is by float or ski equipped fixed wing aircraft or by helicopter.",
65.3925,-107.6817,0,076GSW0064,outcrop,Triangle Lake,076G05,Slave,Au,Undrilled,,,1-Jun-98,Source: Assessment Report,100 Metres,The Triangle Lake Showing is part of the IM 1 Showing (ID 076GSW0063). The IM 1 Showing is approximately 700 m NW along strike.,,
65.3072,-107.5458,0,076GSW0065,outcrop,Orc,076G05,Slave,Zn-Au-Cu,Reconnaissance,,,4-Jun-98,Source: Assessment Report,100 Metres,Location determined by highest assay values.,"The Orc showing is approximately 475 km NE of Yellowknife, NT. Access is by ski or float equipped fixed wing aircraft.",
65.2881,-107.4669,0,076GSW0028,outcrop,KG-97A,076G06,Slave,Au,Reconnaissance,,,18-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given are taken from the sample sites of the map accompanying assessment report 081930. ,"The general area of the sample site is approximately 475 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter",
65.2608,-107.3053,0,076GSW0029,outcrop,KG-117 & KG-140,076G06,Slave,Au,Reconnaissance,,,18-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given are from the highest gold value sample site of the map accompanying assessment report 081930. ,"The showing site is approximately 475 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter",
65.3203,-107.1622,0,076GSW0030,outcrop,Dior,076G06,Slave,Au,Reconnaissance,,,18-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude is from a single sample site that makes up this gold showing. ,"The sample site is approximately 475 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter",
65.3239,-107.1344,0,076GSW0031,outcrop,Sed,076G06,Slave,Au,Reconnaissance,,,18-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude is from the site of the highest gold value.,"The showing site is approximately 475 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter",AR #82966 states that the metamorphic grade varies from greenshist to amphibole within the sedimentary package
65.4378,-107.0317,0,076GSW0032,outcrop,Gersdorffite,076G06,Slave,Ni-Cu-Pd,Undrilled,,,30-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given are taken from the sample sites of the map accompanying assessment report 082070.  ,"The showing site is approximately 475 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter. ",
65.4525,-106.6758,0,076GSE0007,outcrop,Burnside,076G07,Slave,Au,Drilled,,,13-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given is the site of the highest assay value in the showing area.,"The Burnside showing is located approximately 500 km northeast of Yellowknife, NT. The community of Bathurst Inlet is 150 km to the north, and the Lupin mine site is 200 km to the west.  The property is accessible by ski or float equipped fixed wing aircraft or by helicopter.",
65.4811,-107.8467,0,076GSE0008,outcrop,Skarn,076G07,Slave,Au,Reconnaissance,,,17-Mar-98,Source: Assessment Report,30 Metres,The latitude and longitude given is the site of the highest of the highest gold value in the showing area. ,"The Skarn showing is located approximately 500 km northeast of Yellowknife, NT. The community of Bathurst Inlet is 150 km to the north, and the Lupin minesite is 200 km to the west.  The property is accessable by ski or float equipped fixed wing aircraft or by helicopter.",
65.7519,-106.4044,0,076GNE0006,outcrop,Ellice River,076G09,Slave,Au,Drilled,,,9-Jan-98,Source: Assessment Report,30 Metres,The Ellice River area lies within the Back River Region and consists of the Ellice and Eagle occurrences. The Eagle occurrence is within the Contact-Hawk Lakes area. The latitude and longitude given is the point with the highest assay values.,"The Ellice River area and the Boot Lake area both lie within the Back River Region which is approximately 510 km northeast of Yellowknife, the Lupin Mine at Contoyto Lake is approximately 215 km to the west. The centre of the Ellice River area is approximately 7.5 km from the Boot Lake campsite. Access to the area is by float or ski equipped fixed wing planes or by helicopter to Boot Lake. Tundra wheeled Twin Otter can utilize an unimproved esker during the summer months.","The Beachey Lake Group sedimentary rocks, including the oxide iron formations, within the Ellice-Rooster-Boot Property have been deformed into a broad Z shape extending from Scorpion Lake (approximately 5 km to the SW)to Hammer Lake (approximately 11.5 km to the SE). The Boot Lake granitic stock (located south of Boot Lake approximately 7.5 km to the SSW), intrudes this stratigraphy but is not believed to be responsible for the folding. The Z structure may be the result of two regional scale fold systems (Chandler et al, 1992). The regional metamorphism of the Yellowknife Supergroup in this area generally ranges from lower greenschist to lower amphibolite. It reaches upper amphibolite proximal to late Archean felsic intrusives."
65.6992,-106.4772,0,076GNE0010,outcrop,Boot Lake,076G09,Slave,Au,Drilled,,,30-Jan-98,Source: Assessment Report,30 Metres,"The Boot Lake Showing is in oxide and silicate iron formation which lies within the Back River Region. The Boot Lake area consists of numerous mineral occurances including: Chick Pond, Ayers, Aiomon, Aiomon West, Poison Pond, Boot West, Boot Lake North, Spur, Grizzly, Eon, Sunset, Jigsaw, Auk, Dogbone, Links, LR, Cumquat, DO, Toby, and the Plota. The latitude and longitude given is the site of the best gold values.   ","The approximate centre of the Boot Lake area is 1.8 km from the Boot Lake Camp. The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski equipped light aircraft. Tundra wheeled Twin Otter aircraft can utilize an unimproved esker airstrip in the summer. ","The Boot Lake sediments have a metamorphic grade of upper greenschist facies except in the 250 to 300 m contact metamorphic aureole that surrounds the Boot Lake stock (situated approximately 2 km S from the centre of the Boot Lake showing). In that area the regional metamorphic grade is overprinted to lower amphibolite facies (Williamson et al, 1991)."
65.6567,-106.4283,0,076GNE0011,outcrop,Winter,076G09,Slave,Au,Undrilled,,,30-Jan-98,Source: Assessment Report,30 Metres,The Winter Showing is a gold showing hosted by oxide and silicate iron formation which lies within the Back River Region.  The latitude and longitude is the site of the highest assay value.   ,"The approximate centre of the Winter Showing is 3.3 km from the Boot Lake Camp (situated on the north shore of Boot Lake). The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski equipped light aircraft. Tundra wheeled Twin Otter aircraft can utilize an unimproved esker airstrip in the summer. ","The Boot Lake Area sediments have a metamorphic grade of upper greenschist facies except in the 250 to 300 m contact metamorphic aureole that surrounds the Boot Lake stock. In that area the regional metamorphic grade is overprinted to lower amphibolite facies (Williamson et al, 1991). "
65.6542,-106.2903,0,076GNE0012,outcrop,Rooster-Hammer,076G09,Slave,Au,Drilled,,,30-Jan-98,Source: Assessment Report,30 Metres,"The Rooster-Hammer Showing is a gold showing hosted by oxide and silicate iron formation which lies within the Back River region. The Rooster-Hammer Showing is composed of the Rooster, Hammer, Fox Pond, Falcon Creek and Falcon Creek North occurences. The latitude and longitude given is the approximate centre of the Hammer occurence.  ","The approximate centre of the Rooster-Hammer Area is about 7 km from the Boot Lake Camp. The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski equipped light aircraft. Tundra wheeled Twin Otter aircraft can utilize an unimproved esker airstrip in the summer.  ",The Rooster-Hammer area sediments have a metamorphic grade of upper greenschist facies.
65.7469,-106.4456,0,076GNE0013,outcrop,Dumbo Lake,076G09,Slave,Au,Undrilled,,,9-Feb-98,Source: Assessment Report,1000 Metres,The Dumbo Lake Showing latitude and longitude location is the site of the highest gold values.,"The approximate centre of the Dumbo Lake area is 5.3 km NE from the Boot Lake Camp (located on the north shore of Boot Lake). The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski equipped light aircraft. Tundra wheeled Twin Otter aircraft can utilize an unimproved esker airstrip in the summer.   ",The sedimentary rocks of the Dumbo Lake area have a metamorphic grade ranging from greenschist to upper greenschist adjacent to a granitic sill.
65.6658,-106.3475,0,076GNE0014,outcrop,Shell Lake,076G09,Slave,Au,Undrilled,,,20-Feb-98,Source: Assessment Report,30 Metres,The Shell Lake Showing latitude and longitude location is the site of the highest gold values. ,"The approximate centre of the Shell Lake area is 7 km SE of the Boot Lake Camp (located on the north shore of Boot Lake). The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski equipped light aircraft. Tundra wheeled Twin Otter aircraft can utilize an unimproved esker airstrip in the summer.   ",
65.5439,-106.4278,0,076GNE0017,outcrop,Goose Lake,076G09,Slave,Au,Resources Calculated,,,24-Feb-98,Source: Assessment Report,30 Metres,The latitude and longitude given is the site of the highest gold values of the showing area.,"Goose Lake is approximately 15 km south of Boot Lake Camp. THe property is approximately 500 km NE of Yellowknife, NT. Access is available by either float or ski equipped light aircraft to Goose Lake. In summer, tundra wheeled Twin Otter aircraft can utilize an undeveloped esker on the west side of Goose Lake.",The iron formation has been complexly folded and has a metamorphic grade is middle greenschist to lower amphibolite.
65.5456,-106.4564,0,076GNE0018,outcrop,Goose Neck,076G09,Slave,Au,Reconnaissance,,,25-Feb-98,Source: Assessment Report,30 Metres,The latitude and longitude given is the site of the highest gold value for the showing area. ,"Goose Neck is approximately 15 km south of Boot Lake Camp. The property is approximately 500 km NE of Yellowknife, NT. Access is available by either float or ski equipped light aircraft to Goose Lake. In summer, tundra wheeled Twin Otter aircraft can utilize an undeveloped esker on the west side of Goose Lake. ",An airborne geophysical survey shows complex folding and faulting exists in the Goose Neck area.
65.7394,-106.5269,0,076GNE0007,outcrop,Trout Lake,076G10,Slave,Au,Undrilled,,,28-Jan-98,Source: Assessment Report,30 Metres,The Trout Lake Showing lies within the Back River Region. The latitude and longitude given is the site of the highest assay value.,"Trout lake is located approximately 6.5 km northwest of the Boot Lake Camp. The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski equipped light aircraft. Tundra wheeled Twin Otter aircraft can utilize an unimproved esker airstrip in the summer.","At least four periods of deformation have affected the rocks of the Yellowknife Supergroup (Chandler et al, 1992). The Beachey Lake Group sedimentary rocks, including the oxide iron formations, within the Ellice-Rooster-Boot Property have been deformed into a broad Z shape extending from Scorpion Lake (approximately 1.4 km to the SW of the centre of the Trout Lake area) to Hammer Lake (approximately 14.5 km to the SE). The Boot Lake granitic stock (located south of Boot Lake approximately 8.5 km to the SSE), intrudes this stratigraphy but is not believed to be responsible for the folding. The Z structure may be the result of two regional scale fold systems (Chandler et al, 1992). The Trout Lake showing is believed to be an extension of the Scorpion Lake North showing the centre of which is approximately 2.6 km south. The regional metamorphism of the Yellowknife Supergroup in this area is greenschist.  "
65.7181,-106.5192,0,076GNE0008,outcrop,Scorpion Lake North,076G10,Slave,Au,Drilled,,,29-Jan-98,Source: Assessment Report,30 Metres,The Scorpion Lake North Showing is in oxide and silicate iron formation on the southwest shore of Scorpion Lake which lies within the Back River Region and is an extension of the Boot Lake Showing. The latitude and longitude are from the area of the highest assay values.,"Scorpion Lake North is located approximately 5 km northwest of the Boot Lake Camp. The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski equipped light aircraft. Tundra wheeled Twin Otter aircraft can utilize an unimproved esker airstrip in the summer. ","The Beechy Lake Group sedimentary rocks, including the oxide iron formations, within the Ellice-Rooster-Boot Property have been deformed into a broad Z shape extending from Scorpion to Hammer Lake. The Boot Lake granitic stock (located south of Boot Lake), intrudes this stratigraphy but is not believed to be responsible for the folding. The Z structure may be the result of two regional scale fold systems (Chandler et al, 1992).  The regional metamorphism of the Yellowknife Supergroup in this area generally ranges from lower greenschist to lower amphibolite. It reaches upper amphibolite proximal to late Archean felsic intrusives.  "
65.7078,-106.5053,0,076GNE0009,outcrop,Scorpion Lake,076G10,Slave,Au,Drilled,,,29-Jan-98,Source: Assessment Report,30 Metres,The Scorpion Lake showing is in oxide and silicate iron formation on the southwest shore of Scorpion Lake which lies within the Back River Region and is an extension of the Boot Lake Showing. The latitude and longitude given is the site of the highest gold value.  ,"Scorpion Lake is located approximately 3.5 km northwest of the Boot Lake Camp. The Boot Lake property is approximately 500 km northeast of Yellowknife, NT. Access to the camp on Boot Lake is via float or ski equipped light aircraft. Tundra wheeled Twin Otter aircraft can utilize an unimproved esker airstrip in the summer. ","The Beachy Lake Group sedimentary rocks, including the oxide iron formations, within the Ellis-Rooster-Boot Property have been deformed into a broad Z shape extending from Scorpion to Hammer Lake. The Boot Lake granitic stock (located south of Boot Lake), intrudes this stratigraphy but is not believed to be responsible for the folding. The Z structure may be the result of two regional scale fold systems (Chandler et al, 1992).  The regional metamorphism of the Yellowknife Supergroup in this area generally ranges from lower greenschist to lower amphibolite. It reaches upper amphibolite proximal to late Archean felsic intrusives. "
65.6642,-106.9086,0,076GNE0015,outcrop,Boulder Pond,076G10,Slave,Au,Drilled,,,23-Feb-98,Source: Assessment Report,30 Metres,"The latitude and longitude are the site of the highest gold values of the Boulder Lake area which includes the following gold occurences: East Boulder Pond, West Boulder Pond, Peace Lake, Opener Lake, Porkchop, Jaeger, Player, 4DHZ004 and Humpback.","The approximate centre of the Boulder Pond area is about 37.6 km SE of the George Lake Camp. The property is approximately 500 km northeast of Yellowknife, NT. and 150 km south of the community of Bathurst Inlet. The property is accessable by float or ski plane to several of the lakes within the area.",Abundant chlorite indicates that this area has undergone upper greenschist facies metamorphism.  Coarse grained euhedral magnetite porphyroblasts replace chlorite within zones of intense alteration of the oxide iron formation. Howe(1993)suggests this may indicate retrograde metamorphism.
65.6253,-106.8775,0,076GNE0016,outcrop,Soi Lake,076G10,Slave,Au,Undrilled,,,24-Feb-98,Source: Assessment Report,30 Metres,The latitude and longitude are taken from the site of the highest gold value in the Soi Lake area.,"The approximate centre of the Soi Lake area is about 41 km SE of the George Lake Camp. The property is approximately 500 km northeast of Yellowknife, NT. and 150 km south of the community of Bathurst Inlet. The property is accessable by float or ski plane to several of the lakes within the area. ","South of Soi Lake the Vega oxide iron formation is 70-80 m wide and extends 200 m south where it terminates adjacent to a 60 m wide NW trending gabbroic dyke. This termination may be due to a fold closure, this is indicated by repetative outcrop scale isoclinal folds. Ground magnetic data from 1987 indicates that the Soi Lake iron formation exists in a regional sized isoclinal fold."
65.5492,-106.5058,0,076GNE0019,outcrop,Goose Creek,076G10,Slave,Au,Undrilled,,,25-Feb-98,Source: Assessment Report,30 Metres,The latitude and longitude given is the site of the highest gold value for the showing area.   ,"Goose Creek is approximately 15 km south of Boot Lake Camp. The property is approximately 500 km NE of Yellowknife, NT. Access is available by either float or ski equipped light aircraft to Goose Lake. In summer, tundra wheeled Twin Otter aircraft can utilize an undeveloped esker on the west side of Goose Lake.  ",Ground and airborne magnetic surveys indicate that the sedimentary sequence of the Goose Creek area is folded into a large S configuration.
65.5711,-106.55,0,076GNE0020,outcrop,Llama Lake,076G10,Slave,Au,Undrilled,,,25-Feb-98,Source: Assessment Report,30 Metres,The latitude and longitude given is the site of the highest gold value in the showing area.  ,"Llama Lake is approximately 15 km south of Boot Lake Camp. The property is approximately 500 km NE of Yellowknife, NT. Access is available by either float or ski equipped light aircraft to Goose Lake. In summer, tundra wheeled Twin Otter aircraft can utilize an undeveloped esker on the west side of Goose Lake.  ",West of Llama Lake approximately 1.5 km a granitic pluton intrudes the sediments. Cordiorite within a biotite schist about 800 m west of Llama Lake indicates that the sediments have been metamorphosed to lower amphibolite grade near the pluton.  Ground magnetic data indicates that oxide iron formation is complexly folded near and beneath Llama Lake.
65.5722,-107.4061,0,076GNW0014,outcrop,Knight,076G11,Slave,Au,Reconnaissance,,,7-Apr-98,Source: Assessment Report,100 Metres,The location is the sample site of sample 421-1 from assessment report 082070 map 6/7,"The Knight occurrence is approximately 500 km NE of Yellowknife, NT. Access is by ski or float equipped fixed wing airplane or by helicopter.",
65.6044,-107.9383,0,076GNW0002,outcrop,Yava,076G12,Slave,Zn-Cu-Ag-Pb-Au,Drilled,159300,076G12ZN 001,22-Oct-97,Source: Assessment Report,100 Metres,"The Yava Showing has been cited in numerous references as having drill-indicated reserves of 1,000,000 to 2,000,000 tonnes grading 3% Zn, 0.5% Cu, 0.5% Pb, 102.8 g/t (or 10%) Ag and 2 g/t Au. It is difficult to determine what these figures are based on, and the only conclusion which presents itself is that they are based on the 8 mineralized intersections of the 1974-75 drill program - or more accurately, on speculation regarding these intersections.  Accordingly, this Showing has been assigned a Development Stage of ""Drilled"" rather than ""Resources Calculated"". See Capsule Geology for more information.","The Yava deposit is located 472 km northeast of Yellowknife, NWT, from which point it may be reached by float/ski-equipped fixed wing aircraft or helicopter.",
65.5103,-107.8075,0,076GNW0018,outcrop,Gaet 3,076G12,Slave,Au,Reconnaissance,,,3-Jun-98,Source: Assessment Report,30 Metres,The latitude and longitude are the coordinates of the single sample that make up this showing.,"Gaet 3 is located approximately 460 km NE of Yellowknife, NT. The showing area is accessable  by ski or float equipped fixed wing aircraft.",
65.5294,-107.8186,0,076GNW0019,outcrop,Trumpet,076G12,Slave,Au,Undrilled,,,4-Jun-98,Source: Assessment Report,100 Metres,"The Trumpet showing has three ""satellite"" showings associated with it: 076GNW0020 (the Oboe Showing is approximately 850 m NNE of the Trumpet Showing) , 076GNW0021 (the Flute Showing is approximately 500 m SSE of the Trumpet) & 076GNW0022 (the Picallo Showing is approximately 800 m SSE of the Trumpet).  Latitude and longitude locations is of the best assay value.","The Trumpet showing is located approximately 460 km NE of Yellowknife, NT. Access is by ski or float equipped fixed wing aircraft.",Metamorphosed to greenschist-biotite grade
65.5219,-107.8114,0,076GNW0020,outcrop,Oboe,076G12,Slave,Au,Undrilled,,,4-Jun-98,Source: Assessment Report,30 Metres,,,
65.5364,-107.8142,0,076GNW0021,outcrop,Piccalo,076G12,Slave,Au,Undrilled,,,8-Jun-98,Source: Assessment Report,100 Metres,,,
65.5328,-107.8164,0,076GNW0022,outcrop,Flute,076G12,Slave,Au,Undrilled,,,8-Jun-98,Source: Assessment Report,30 Metres,,,
65.6375,-107.9408,0,076GNW0023,outcrop,Buck,076G12,Slave,Au,Drilled,,,8-Jun-98,Source: Assessment Report,30 Metres,"Latitude and longitude mark the highest concentration of drilling and the best gold values. This showing has two ""satellite"" showings associated with it - the Buck North (076GNW0024) 800 m to the north along strike & the Chopin Showing (076GNW0025) which is approximately 400 m north of the Buck North Showing along strike.","The Buck showing is located approximately 480 km NE of Yellowknife, NT and is accessable by float or ski equipped fixed wing aircraft.",Greenschist-biotite facies
65.6456,-107.9439,0,076GNW0024,outcrop,Buck North,076G12,Slave,Au,Undrilled,,,11-Jun-98,Source: Assessment Report,100 Metres,,,
65.6542,-107.9508,0,076GNW0025,outcrop,Chopin,076G12,Slave,Au,Drilled,,,11-Jun-98,Source: Assessment Report,100 Metres,,,
65.6833,-107.9344,0,076GNW0026,outcrop,Lin,076G12,Slave,Au,Undrilled,,,12-Jun-98,Source: Assessment Report,100 Metres,Latitude and longitude are from the location of the highest assay value.,"The Lin showing is located approximately 460 km NE of Yellowknife, NT and is accessable by float or ski equipped fixed wing aircraft.","Regionally, metamorphic facies fall within this range."
65.69,-107.9308,0,076GNW0027,outcrop,Mozart,076G12,Slave,Au,Reconnaissance,,,12-Jun-98,Source: Assessment Report,100 Metres,The latitude and longitude for the showing is based on the highest gold values.,"The Mozart showing is located approximately 460 km NE of Yellowknife, NT. The showing is accessable by ski or float equipped fixed wing aircraft.",
65.6836,-107.9881,0,076GNW0028,outcrop,Bach,076G12,Slave,Au,Undrilled,,,12-Jun-98,Source: Assessment Report,100 Metres,Latitude and longitude are from the area of highest gold values from a silicate and/or oxide iron formation within greywacke turbidites.,"The Bach Showing is approximately 460 km NE of Yellowknife, NT. The showing area is accessable by float or ski equipped fixed wing aircraft.",Sediments are metamorphosed to at least greenschist facies - biotite grade
65.7144,-107.9392,0,076GNW0029,outcrop,Lin 1,076G12,Slave,Au,Reconnaissance,,,15-Jun-98,Source: Assessment Report,100 Metres,This showing is from a single reconnaissance sample that is located on map 3a of AR 082994. It is noted that this sample was located from previous reconnaissance work.,"The Lin 1 showing is approximately 470 km NE of Yellowknife, NT and is accessable by either float or ski equipped fixed wing aircraft.",
65.7094,-107.9353,0,076GNW0030,outcrop,Lin 2,076G12,Slave,Au,Reconnaissance,,,15-Jun-98,Source: Assessment Report,100 Metres,This showing is from a single reconnaissance sample.,"The Lin 2 showing is approximately 460 km NE of Yellowknife, NT and is accessable by either float or ski equipped fixed wing aircraft.",
65.5925,-107.8836,0,076GNW0031,outcrop,WL1,076G12,Slave,Au,Undrilled,,,15-Jun-98,Source: Assessment Report,100 Metres,Latitude and longitude are determined by the site of the best gold value.,"The WL1 showing is approximately 465 km NE of Yellowknife, Nt and is accessable by either ski or float equipped fixed wing aircraft.",
65.6008,-107.9025,0,076GNW0032,outcrop,Nuts,076G12,Slave,Au,Reconnaissance,,,15-Jun-98,Source: Assessment Report,100 Metres,This showing consists of 2 reconnaissance samples.,"The Nuts showing is located approximately 460 km NE of Yellowknife, NT. Access is by fixed wing aircraft equipped with either skis or floats.",
65.6978,-107.8997,0,076GNW0033,outcrop,51536,076G12,Slave,Au,Reconnaissance,,,15-Jun-98,Source: Assessment Report,100 Metres,This showing consists of a single reconnaissance sample,,
65.6894,-107.895,0,076GNW0034,outcrop,51535,076G12,Slave,Au,Reconnaissance,,,16-Jun-98,Source: Assessment Report,100 Metres,This showing is a single reconnaissance sample that had a gold value of 0.51 g/tonne.,,
65.4947,-107.7622,0,076GSW0033,outcrop,Gaet,076G12,Slave,Au,Undrilled,,,15-Apr-98,Source: Assessment Report,500 Metres,The latitude and longitude given are taken from the sample sites of the map accompanying assessment report 083071. The area discussed is the central area of a grid that is 3 km long by 2 km wide and has the best assay results.,"The general area of the sample site is approximately 450 km NE of Yellowknife, NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.  ",
65.9258,-107.4764,0,076GNW0003,outcrop,George Lake,076G13,Slave,Au,Resources Calculated,,,7-Jan-98,Source: Assessment Report,30 Metres,"The NTS location is determined by selecting an approximate midpoint of the George Lake area.  The George Lake Showing is comprised of 5 deposits and several occurences. The deposits include: Lone Cow Pond, Occurrence Lake (formerly Local 2), George Lake North (formerly locale 1 North, Locale 1), Esker Pond (formerly GH, GH SW, GH Central) and Slave. Occurrences include: Point, Plane, Fold Nose, Forest, Locale 3, Locale 4, Dragon Lake,  and Creek.  ","Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by float or ski equipped fixed wing aircraft or by tundra wheeled Twin Otter to a 250 m airstrip adjacent to the George Lake camp.","Chandler & Holmberg(1990)note that there are several periods of deformation in the George Lake area including ones post dating gold mineralization. NW trending brittle faults to ductile shears trend subparallel to Archean stratigraphy. Stratigraphy is offset by late N-NE conjugate brittle faults.   Folding in the George Lake area is fairly extensive with ""tight to near isoclinal folds, steep west dipping axial planes and and subhorizontal fold axes. This fold geometry is interpretted to be the result of refolding of an earlier fold event such that fold noses exhibit variable attitudes, plunging moderately to steeply towards both the northwest and southeast. A later deformation episode has imposed a mild open warping along north to northeasterly axes with pronounced kink foliation developed in places."" Chandler & Holmberg,1990  The metamorphic grade of the George Lake areas is lower to middle greenschist with chlorite being common and biotite developed in some mudstones."
65.8808,-107.49,0,076GNW0017,outcrop,Dex,076G13,Slave,Au,Undrilled,,,15-Apr-98,Source: Assessment Report,30 Metres,The showing location is centred on the area of best assay data from assessment report 083071.,The Dex showing is approximately 450 km NE of Yellowknife NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.,Greywackes of the showing area are relatively unmetamorphosed.
65.9258,-107.4764,0,076GNW0003,outcrop,George Lake,076G14,Slave,Au,Resources Calculated,,,7-Jan-98,Source: Assessment Report,30 Metres,"The NTS location is determined by selecting an approximate midpoint of the George Lake area.  The George Lake Showing is comprised of 5 deposits and several occurences. The deposits include: Lone Cow Pond, Occurrence Lake (formerly Local 2), George Lake North (formerly locale 1 North, Locale 1), Esker Pond (formerly GH, GH SW, GH Central) and Slave. Occurrences include: Point, Plane, Fold Nose, Forest, Locale 3, Locale 4, Dragon Lake,  and Creek.  ","Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by float or ski equipped fixed wing aircraft or by tundra wheeled Twin Otter to a 250 m airstrip adjacent to the George Lake camp.","Chandler & Holmberg(1990)note that there are several periods of deformation in the George Lake area including ones post dating gold mineralization. NW trending brittle faults to ductile shears trend subparallel to Archean stratigraphy. Stratigraphy is offset by late N-NE conjugate brittle faults.   Folding in the George Lake area is fairly extensive with ""tight to near isoclinal folds, steep west dipping axial planes and and subhorizontal fold axes. This fold geometry is interpretted to be the result of refolding of an earlier fold event such that fold noses exhibit variable attitudes, plunging moderately to steeply towards both the northwest and southeast. A later deformation episode has imposed a mild open warping along north to northeasterly axes with pronounced kink foliation developed in places."" Chandler & Holmberg,1990  The metamorphic grade of the George Lake areas is lower to middle greenschist with chlorite being common and biotite developed in some mudstones."
65.8764,-107.2864,0,076GNW0004,outcrop,Rifle Lake,076G14,Slave,Au,Drilled,,,12-Feb-98,Source: Assessment Report,500 Metres,The Latitude and longitude given is the site of the highest gold value.,"Rifle Lake is in the SW section of the George Lake area, approximately 9.2 km from the George Lake Camp (SW shore of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by float or ski equipped fixed wing aircraft or by tundra wheeled Twin Otter to a 250 m airstrip adjacent to the George Lake camp. ",The NW section of the Rifle Lake area is highly folded forming a SE plunging syncline. Fold closures have an average plunge of 65 degrees SE.
65.8708,-107.3625,0,076GNW0005,outcrop,Komatik Lake,076G14,Slave,Au,Undrilled,,,16-Feb-98,Source: Assessment Report,500 Metres,The Latitude and longitude given is the site of the highest gold value.of the Komatik Lake occurrence on the SSW end of Komatik Lake.,"The Komatik Lake area is Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by float or ski equipped fixed wing aircraft or by tundra wheeled Twin Otter to a 250 m airstrip adjacent to the George Lake camp. ",
65.8678,-107.3447,0,076GNW0006,outcrop,Mouse,076G14,Slave,Au,Undrilled,,,16-Feb-98,Source: Assessment Report,30 Metres,The latitude and longitude are measured from the site of the highest assay of the Mouse showing along strike of the George Lake belt.,"The Mouse showing is within the George Lake belt and is approximately 7.8 km SE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by float or ski equipped fixed wing aircraft or by tundra wheeled Twin Otter to a 250 m airstrip adjacent to the George Lake camp.  ",
65.8667,-107.3094,0,076GNW0007,outcrop,Bullwinkle Lake,076G14,Slave,Au,Undrilled,,,16-Feb-98,Source: Assessment Report,30 Metres,The latitude and longitude are measured from the site of the highest assay value of the Bullwinkle showing along strike of the Fold Nose belt of the George Lake area. ,"The Bullwinkle showing is within the Fold Nose belt of the George Lake area and is approximately 9 km SE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by float or ski equipped fixed wing aircraft or by tundra wheeled Twin Otter to a 250 m airstrip adjacent to the George Lake camp.   ",
65.8786,-107.3678,0,076GNW0008,outcrop,Takrark Lake,076G14,Slave,Au,Undrilled,,,17-Feb-98,Source: Assessment Report,30 Metres,The latitude and longitude are measured from the site of the highest gold value of the Takrark Lake Showing along strike of the Fold Nose belt of the George Lake area.  ,"The Takrark Lake showing is within the Fold Nose belt of the George Lake area and is approximately 5.4 km SE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by float or ski equipped fixed wing aircraft or by tundra wheeled Twin Otter to a 250 m airstrip adjacent to the George Lake camp.    ",
65.8614,-107.2664,0,076GNW0009,outcrop,4LBZ005,076G14,Slave,Au,Reconnaissance,,,17-Feb-98,Source: Assessment Report,30 Metres,The latitude and longitude are measured from the site of the 4LBZ005 sample along strike of the Lookout Hill belt of the George Lake area. ,"The 4LBZ005 showing is within the Lookout Hill belt of the George Lake area and is approximately 10.8 km SE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by float or ski equipped fixed wing aircraft or by tundra wheeled Twin Otter to a 250 m airstrip adjacent to the George Lake camp. ",
65.8522,-107.27,0,076GNW0010,outcrop,West Rapids,076G14,Slave,Au,Reconnaissance,,,18-Feb-98,Source: Assessment Report,30 Metres,The latitude and longitude are measured from the site of the highest assay value of the West Rapids showing along strike of the Fold Nose belt of the George Lake area. ,"The West Rapids showing runs along strike of the Fold Nose belt of the George Lake area and is approximately 11.3 km SE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by float or ski equipped fixed wing aircraft or by tundra wheeled Twin Otter to a 250 m airstrip adjacent to the George Lake camp.  ",
65.8383,-107.2489,0,076GNW0011,outcrop,Oar Lake,076G14,Slave,Au,Drilled,,,18-Feb-98,Source: Assessment Report,30 Metres,The latitude and longitude are measured from the site of the highest gold value of the Oar Lake showing along strike of the Lookout Hill belt of the George Lake area.  ,"The Oar Lake showing runs along strike of the Lookout Hill belt of the George Lake area and is approximately 12.4 km SE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by float or ski equipped fixed wing aircraft or by tundra wheeled Twin Otter to a 250 m airstrip adjacent to the George Lake camp.  ","The iron formation is structurally complex with minor folds, faults and crosscutting quartz veins."
65.9131,-107.3861,0,076GNW0012,outcrop,Shadow Pond,076G14,Slave,Au,Undrilled,,,18-Feb-98,Source: Assessment Report,30 Metres,The latitude and longitude are the site of the highest gold value of the Shadow Pond Showing which lies along strike of the Lookout Hill belt of the George Lake area. ,"The Shadow Pond showing runs along strike of the Lookout Hill belt of the George Lake area and is approximately 3.4 km NE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by float or ski equipped fixed wing aircraft or by tundra wheeled Twin Otter to a 250 m airstrip adjacent to the George Lake camp.  ",Steeply dipping SW trending faults cut through the area with displacements up to 200 m.
65.9303,-107.4203,0,076GNW0013,outcrop,Lookout Hill,076G14,Slave,Au,Drilled,,,18-Feb-98,Source: Assessment Report,30 Metres,The latitude and longitude are measured from the site of the highest gold value of the Lookout Hill showing which lies along strike of the Lookout Hill belt of the George Lake area. ,"The Lookout Hill showing runs along strike of the Lookout Hill belt of the George Lake area and is approximately 2 km ENE of George Lake Camp (located on the SW tip of George Lake). Yellowknife, NT is approximately 515 km SW of the approximate centre of the George Lake area. Access to the area is by float or ski equipped fixed wing aircraft or by tundra wheeled Twin Otter to a 250 m airstrip adjacent to the George Lake camp. ",Steeply dipping SW trending faults cut through the Lookout Hill area.
65.9356,-107.3942,0,076GNW0015,outcrop,U-1,076G14,Bear,U-Au-Pb,Undrilled,,,8-Apr-98,Source: Assessment Report,1000 Metres,The U-1 showing location is from a sample location marked on map 5 from assessment report 081178. The sample sites are clearly marked but there are no corresponding sample numbers. The assessment report does state that the samples are from this area.,"The U-1 showing is located approximately 500 km NE of Yellowknife, NT. The area is accessable by float or ski equipped fixed wing aircraft.","The Goulburn Group has been folded - intensity varies with competancy. The Western River Formation is tightly folded, less competant and the Burnside Formation drapes over it. Folds have NS axial planes which are vertical or dip steeply east."
65.8267,-107.1078,0,076GNW0016,outcrop,U-2,076G14,Slave,U,Reconnaissance,,,9-Apr-98,Source: Assessment Report,100 Metres,The U-2 showing location is from sample locations marked on map 5 from assessment report 081178. The sample sites are clearly marked but thee are no corresponding sample numbers just listed assay values that are not discussed in the body of the report.,"The U-2 showing is located approximately 500 km NE of Yellowknife, NT. The area is accessable by float or ski equipped fixed wing aircraft. ",Folding and faulting noted.
65.8808,-107.49,0,076GNW0017,outcrop,Dex,076G14,Slave,Au,Undrilled,,,15-Apr-98,Source: Assessment Report,30 Metres,The showing location is centred on the area of best assay data from assessment report 083071.,The Dex showing is approximately 450 km NE of Yellowknife NT. Access to the area is by ski or float equipped fixed wing aircraft or by helicopter.,Greywackes of the showing area are relatively unmetamorphosed.
65.81,-106.4528,0,076GNE0004,outcrop,Western River 1,076G16,Slave,Cu,Observed Ore Mineral,526000,,22-Oct-97,Method: Map/Airphoto,500 Metres,"Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada.  Administrative Region:  District Of Mackenzie  ""Showing"" is nothing more than the presence of chalcopyrite noted on a map.",,
65.7819,-106.4208,0,076GNE0005,outcrop,Western River 2,076G16,Slave,Cu,Observed Ore Mineral,1061300,,22-Oct-97,Method: Map/Airphoto,500 Metres,Record derived from the Canadian Mineral Occurrence Index (CANMINDEX) of the Geological Survey of Canada.  Administrative Region:   District Of Mackenzie,,
65.7519,-106.4044,0,076GNE0006,outcrop,Ellice River,076G16,Slave,Au,Drilled,,,9-Jan-98,Source: Assessment Report,30 Metres,The Ellice River area lies within the Back River Region and consists of the Ellice and Eagle occurrences. The Eagle occurrence is within the Contact-Hawk Lakes area. The latitude and longitude given is the point with the highest assay values.,"The Ellice River area and the Boot Lake area both lie within the Back River Region which is approximately 510 km northeast of Yellowknife, the Lupin Mine at Contoyto Lake is approximately 215 km to the west. The centre of the Ellice River area is approximately 7.5 km from the Boot Lake campsite. Access to the area is by float or ski equipped fixed wing planes or by helicopter to Boot Lake. Tundra wheeled Twin Otter can utilize an unimproved esker during the summer months.","The Beachey Lake Group sedimentary rocks, including the oxide iron formations, within the Ellice-Rooster-Boot Property have been deformed into a broad Z shape extending from Scorpion Lake (approximately 5 km to the SW)to Hammer Lake (approximately 11.5 km to the SE). The Boot Lake granitic stock (located south of Boot Lake approximately 7.5 km to the SSW), intrudes this stratigraphy but is not believed to be responsible for the folding. The Z structure may be the result of two regional scale fold systems (Chandler et al, 1992). The regional metamorphism of the Yellowknife Supergroup in this area generally ranges from lower greenschist to lower amphibolite. It reaches upper amphibolite proximal to late Archean felsic intrusives."